Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ...
The geometries of a catchment constitute the basis for distributed physically based numerical modeling of different geoscientific disciplines. In this paper results from ground-penetrating radar (GPR) measurements, in terms of a 3-D model of total sediment thickness and active layer thickness in a p...
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Online Access: | https://dx.doi.org/10.1594/pangaea.845258 https://doi.pangaea.de/10.1594/PANGAEA.845258 |
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ftdatacite:10.1594/pangaea.845258 2024-09-15T18:08:54+00:00 Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... Petrone, Johannes Sohlenius, Gustav Johansson, Emma Lindborg, Tobias Näslund, Jens-Ove Strömgren, Mårten Brydsten, Lars 2016 application/zip https://dx.doi.org/10.1594/pangaea.845258 https://doi.pangaea.de/10.1594/PANGAEA.845258 en eng PANGAEA https://dx.doi.org/10.5194/essd-8-663-2016 https://dx.doi.org/10.1594/pangaea.836178 https://dx.doi.org/10.1594/pangaea.860961 Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 GReenland Analogue Surface Project GRASP dataset Supplementary Dataset Dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.84525810.5194/essd-8-663-201610.1594/pangaea.83617810.1594/pangaea.860961 2024-08-01T10:57:41Z The geometries of a catchment constitute the basis for distributed physically based numerical modeling of different geoscientific disciplines. In this paper results from ground-penetrating radar (GPR) measurements, in terms of a 3-D model of total sediment thickness and active layer thickness in a periglacial catchment in western Greenland, are presented. Using the topography, the thickness and distribution of sediments are calculated. Vegetation classification and GPR measurements are used to scale active layer thickness from local measurements to catchment-scale models. Annual maximum active layer thickness varies from 0.3 m in wetlands to 2.0 m in barren areas and areas of exposed bedrock. Maximum sediment thickness is estimated to be 12.3 m in the major valleys of the catchment. A method to correlate surface vegetation with active layer thickness is also presented. By using relatively simple methods, such as probing and vegetation classification, it is possible to upscale local point measurements to ... : Supplement to: Petrone, Johannes; Sohlenius, Gustav; Johansson, Emma; Lindborg, Tobias; Näslund, Jens-Ove; Strömgren, Mårten; Brydsten, Lars (2016): Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland. Earth System Science Data, 8(2), 663-677 ... Dataset Greenland DataCite |
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Open Polar |
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op_collection_id |
ftdatacite |
language |
English |
topic |
GReenland Analogue Surface Project GRASP |
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GReenland Analogue Surface Project GRASP Petrone, Johannes Sohlenius, Gustav Johansson, Emma Lindborg, Tobias Näslund, Jens-Ove Strömgren, Mårten Brydsten, Lars Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
topic_facet |
GReenland Analogue Surface Project GRASP |
description |
The geometries of a catchment constitute the basis for distributed physically based numerical modeling of different geoscientific disciplines. In this paper results from ground-penetrating radar (GPR) measurements, in terms of a 3-D model of total sediment thickness and active layer thickness in a periglacial catchment in western Greenland, are presented. Using the topography, the thickness and distribution of sediments are calculated. Vegetation classification and GPR measurements are used to scale active layer thickness from local measurements to catchment-scale models. Annual maximum active layer thickness varies from 0.3 m in wetlands to 2.0 m in barren areas and areas of exposed bedrock. Maximum sediment thickness is estimated to be 12.3 m in the major valleys of the catchment. A method to correlate surface vegetation with active layer thickness is also presented. By using relatively simple methods, such as probing and vegetation classification, it is possible to upscale local point measurements to ... : Supplement to: Petrone, Johannes; Sohlenius, Gustav; Johansson, Emma; Lindborg, Tobias; Näslund, Jens-Ove; Strömgren, Mårten; Brydsten, Lars (2016): Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland. Earth System Science Data, 8(2), 663-677 ... |
format |
Dataset |
author |
Petrone, Johannes Sohlenius, Gustav Johansson, Emma Lindborg, Tobias Näslund, Jens-Ove Strömgren, Mårten Brydsten, Lars |
author_facet |
Petrone, Johannes Sohlenius, Gustav Johansson, Emma Lindborg, Tobias Näslund, Jens-Ove Strömgren, Mårten Brydsten, Lars |
author_sort |
Petrone, Johannes |
title |
Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
title_short |
Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
title_full |
Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
title_fullStr |
Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
title_full_unstemmed |
Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, Western Greenland, link to shapefiles ... |
title_sort |
using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, western greenland, link to shapefiles ... |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.845258 https://doi.pangaea.de/10.1594/PANGAEA.845258 |
genre |
Greenland |
genre_facet |
Greenland |
op_relation |
https://dx.doi.org/10.5194/essd-8-663-2016 https://dx.doi.org/10.1594/pangaea.836178 https://dx.doi.org/10.1594/pangaea.860961 |
op_rights |
Creative Commons Attribution Non Commercial Share Alike 3.0 Unported https://creativecommons.org/licenses/by-nc-sa/3.0/legalcode cc-by-nc-sa-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.84525810.5194/essd-8-663-201610.1594/pangaea.83617810.1594/pangaea.860961 |
_version_ |
1810446275976364032 |